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Fig. 4 in The Chinchilla Local Fauna: An exceptionally rich and well-preserved Pliocene vertebrate assemblage from fluviatile deposits of south-eastern Queensland, Australia

Fig. 4. Reptiles from Chinchilla Sand, Australia, Pliocene. A.?Reptilia, QM F56197, Chinchilla Rifle Range, unidentified fragments (A 1 –A 3), showing the WPC registration numbers of Agamidae sp. indet. cited by Hutchinson and Mackness (2002). B. Varanus sp. QM F56189, "Wilkinson's Quarry" Chinchilla Rifle Range, dorsal vertebra. C. Quinkana sp., QM F10204, Chinchilla Rifle Range, isolated tooth. D. Trionychidae sp. indet. QM F9037, Fairymeadow, carapace fragment. E. Emydura sp., QM F7035, Middle Gully, Chinchilla Rifle Range, anterior half of carapace. F. Pallimnarchus pollens de Vis, 1886, QM F11612, "Sand Scree locality, 4'6" from top of bank of Condamine River", symphyseal portion of dentary. G. Varanus komodoensis Ouwens, 1912, QM F874, unspecified locality near Chinchilla, right maxilla. Scale bars 20 mm.

Fig. 6 in A well-preserved partial skeleton of the poorly known early Miocene seriema Noriegavis santacrucensis

Fig. 6. Strict consensus tree of two most parsimonious tree resulting from analysis of the character matrix in SOM 1 (Supplementary Online Material available at http://app.pan.pl/SOM/app60-Mayr_Noriega_SOM.pdf) length = 55, CI = 0.70, RI = 0.72). Characters (top) and character states bottom) are listed, with filled circles representing unambiguous apomorphies. Bootstrap support values are indicated next to the internodes, fossil taxa are marked with a dagger.

Fig. 2 in A well-preserved partial skeleton of the poorly known early Miocene seriema Noriegavis santacrucensis

Fig. 2. Comparison of skulls and mandibles of the seriema (Cariamidae) Noriegavis santacrucensis (Noriega Vizcaíno, and Bargo, 2009) from the early Miocene Santa Cruz Formation in Argentina (A) with extant Chunga burmeisteri (Hartlaub, 1860) (C) and extant Cariama cristata Bonaparte, 1853 (B, D). A. MPM-PV 15049, skull in left lateral (A 1), right lateral (A 2), dorsal (A 5), and caudal (A 6) views, skull with upper beak oriented in its natural position (A 3); partial mandible in right lateral view (A 4); left os lacrimale in dorsal (A 7) and lateral (A 8) views. B. SMF 1710, skull in dorsal view. C. MACN 2351, skull in dorsal (C 1) and lateral (C 2) views. D. SMF 1862, skull in lateral view.

Fig. 3 in A well-preserved partial skeleton of the poorly known early Miocene seriema Noriegavis santacrucensis

Fig. 3. Wing bones and sternum of the seriema (Cariamidae) Noriegavis santacrucensis (Noriega, Vizcaíno, and Bargo, 2009) from the early Miocene Santa Cruz Formation in Argentina (B), in comparison with extant Cariama cristata Bonaparte, 1853 (A, C). A. SMF 1710, proximal left humerus in cranial view (A 1), proximal right ulna in caudal view (A 2), right phalanx proximalis digiti majoris in ventral view (A 3). B. MPM-PV 15049, proximal half of left humerus in cranial (B 1) and caudal (B 2) views, proximal portion of right ulna in cranial (B 3) and caudal (B 4) views, distal end of left ulna in ventral view (B 5), right phalanx proximalis digiti majoris in ventral view (B 6), sternum in right lateral (B 7) and cranial (B 8) views. C. SMF 2462, sternum in lateral (C 1) and cranial (C 2) views.

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Fig. 1 in The Chinchilla Local Fauna: An exceptionally rich and well-preserved Pliocene vertebrate assemblage from fluviatile deposits of south-eastern Queensland, Australia

Fig. 1. Physiography of the Chinchilla local area, showing the location of Chinchilla relative to the Condamine River System. Redrawn after Reiser 1971).

Fig. 5 in A well-preserved partial skeleton of the poorly known early Miocene seriema Noriegavis santacrucensis

Fig. 5. Hindlimb bones of the seriema (Cariamidae) Noriegavis santacrucensis (Noriega, Vizcaíno, and Bargo, 2009) from the early Miocene Santa Cruz Formation in Argentina (A) in comparison with extant Cariama cristata Bonaparte, 1853 (B–D). A. MPM-PV 15049. B. SMF 1710. C. SMF 2462. D. SMF 1862. Right femur in caudal (A 1, B) and cranial (A 2) views. Right tibiotarsus: cranial view (A 3, C 1), distal end in caudal (A6) and cranial (A 7) views, proximal end in proximal view (A 8, C 2). Left tarsometatarsus: shaft in cranial (A 4) and caudal (A5) views, distal end in dorsal (A 9, D 1), plantar (A 11), and distal (A 14, D 2) views. Right tarsometatarsus in dorsal (A 10) and plantar (A 12) views, pedal phalanges (A 13)

Fig. 1 in A well-preserved partial skeleton of the poorly known early Miocene seriema Noriegavis santacrucensis

Fig. 1. Map of southeastern Patagonia (A) and detail map (B) showing the position of the Monte Tigre locality, from which the new Noriegavis santacrucensis fossil comes, and the holotype locality Punto Estancia La Costa.

Fig. 4 in A well-preserved partial skeleton of the poorly known early Miocene seriema Noriegavis santacrucensis

Fig. 4. Pelvis of the seriema (Cariamidae) Noriegavis santacrucensis (Noriega, Vizcaíno, and Bargo, 2009) from the early Miocene Santa Cruz Formation in Argentina (A) in comparison with extant Cariama cristata Bonaparte, 1853 (B). A. MPM-PV 15049, in ventral (A1), dorsal (A2), and lateral (A3) views, with detail of cristae iliacae dorsales (A4). B. SMF 1862, pelvis in dorsal view (B1) and detail in lateral view (B2).

Fig. 5 in Soft-part preservation in a linguliform brachiopod from the lower Cambrian Wulongqing Formation (Guanshan Fauna) of Yunnan, South China

Fig. 5. Reconstruction of Acanthotretella decaius sp. nov. based on GKG CA−007,GKG CA−008, GKG CA−002B, showing disposition of lophophore, small visceral cavity and location of measurements indicated in Table 1.

Fig. 4 in Soft-part preservation in a linguliform brachiopod from the lower Cambrian Wulongqing Formation (Guanshan Fauna) of Yunnan, South China

Fig. 4. Sketch drawings of the linguliform brachiopod Acanthotretella decaius sp. nov. illustrated in Fig. 2 and 3. A. Sketch of Fig. 2C1 (GKG CA−008B). B. Sketch of Fig. 2 E(GKG CA−002B). C. Sketch of Fig. 3C1(GKG CA−007B). D. Sketch of Fig. 3D1(GKG CA−013(2)). Scale bars 5 mm.

Fig. 1. A in Soft-part preservation in a linguliform brachiopod from the lower Cambrian Wulongqing Formation (Guanshan Fauna) of Yunnan, South China

Fig. 1. A. Map showing the locality (star) where the brachiopod Acanthotretella decaius sp. nov. was collected. B. Stratigraphical correlation of the muddy deposits yielding the Guanshan fanua including A. decaius sp. nov. in Gaoloufang section near Guangwei village, Kunming, southern China.

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Fig. 7. Longitudinal section through the well preserved specimen PIMUZ 28583 in Devonian pearls and ammonoid-endoparasite co-evolution

Fig. 7. Longitudinal section through the well preserved specimen PIMUZ 28583 of Sellanarcestes spp., Sellanarcestes wenkenbachi Zone, Emsian, Oufrane (S of Tata), Morocco. A. +/− median section displaying many "Housean pits", most with internal tube; overview. "Housean pits" are marked by white arrows. B. Three closely spaced pits, two displaying the internal tubes, the remaining void inside the pit is filled with a fine−grained sparitic matrix, note the continuous ammonoid shell layer covering the pits and the septum, which grew on the pit wall, note the distinguishable shell layers, which are recrystallised to varying degrees. C. A corroded pit with tube, note the continuation of the innermost ammonoid shell layer. D. Two adjacent fused pits, only the right pit shows the delicate internal tube, mural part of septum on the left.

Fig. 3 in Soft-part preservation in a linguliform brachiopod from the lower Cambrian Wulongqing Formation (Guanshan Fauna) of Yunnan, South China

Fig. 3. Linguliform brachiopod Acanthotretella decaius sp. nov. from the early Cambrian Guanshan fauna, showing the proximal pedicles (tailed arrows) and gut remains (simple arrows), Yunnan, China. A. GKG CA−014, a muddy slab with two individuals preserved together. B–D. Photographs showing the U−shaped digestive tracts preserved as tubular imprints (simple arrows) with some relief. B. GKG CA−011B. C. GKG CA−007B. D. GKG CA−013(2). General view (C1, D1), close−up (C2, D2) of tubular relief of guts. See Fig. 4 for interpretations of C1 and D1.

Fig. 2 in Soft-part preservation in a linguliform brachiopod from the lower Cambrian Wulongqing Formation (Guanshan Fauna) of Yunnan, South China

Fig. 2. Linguliform brachiopod Acanthotretella decaius sp. nov. from the Wulongqing Formation (Palaeolenus Zone), lower Cambrian (recently Series 2, Stage 4), China. A. Holotype, GKG CA−007 in general view (A1); posterior details of the shell valves (A2), showing the small body cavity posteromedially placed, the elongate subtriangular pseudointerarea and the proximate pedicle; details of the gentle S−shaped portion of pedicle in A1 (A3); close−up view of the pedicle annulations in A1 (A4). B. GKG CA−008A, a flattened specimen anterolaterally compressed in general view (B1), showing the concentric growth +

Fig. 2 in Unusual environmental conditions preserve a Permian mesosaur-bearing Konservat-Lagerstätte from Uruguay

Fig. 2. Mesosaurid scapulocoracoid, FC−DPV 2493, part (A) and counterpart (B), from the Early Permian Mangrullo Formation (Northeastern Uruguay) preserved in a shale surface highly bioturbated by the trace fossil Chondrites.

Fig. 1 in Unusual environmental conditions preserve a Permian mesosaur-bearing Konservat-Lagerstätte from Uruguay

Fig. 1. Generalized stratigraphic section of the Early Permian Mangrullo Formation (Northeastern, Uruguay), showing the various sedimentary facies and their corresponding fossil associations, including the "mesosaur community". Colour codes from standard Munsell Chart. Abbreviations: C, conglomerate; S, silt; FS, fine sandstone.

Fig. 9 in Unusual environmental conditions preserve a Permian mesosaur-bearing Konservat-Lagerstätte from Uruguay

Fig. 9. Exceptional preservation of internal anatomy in Mesosaurus tenuidens (FC−DPV 2109) from the Early Permian Mangrullo Formation (Northeastern Uruguay). Photograph (A) and interpretive drawing (B) of the internal mould of articulated mandibular rami, showing well preserved mandibular nerves, probably the trigeminus ramus, running along the dentary tooth series (black arrow in B), and delicate blood vessels (grey arrow in B).

Fig. 6 in Unusual environmental conditions preserve a Permian mesosaur-bearing Konservat-Lagerstätte from Uruguay

Fig. 6. Gypsum crystals from the Early Permian Mangrullo Formation (Norteastern Uruguay). A. FC−DPV 2518, gypsum crystals surrounding a mesosaur skeleton. B. GMHR 0001, gypsum crystals associated with oil−shale deposits, with interpretive drawing of crystals in the left corner. C. GMHR 0002, impressions of the crystals found in non−bituminous shale. D. GMHR 0003, columnar gypsum crystals from bituminous shales.

Fig. 8 in Unusual environmental conditions preserve a Permian mesosaur-bearing Konservat-Lagerstätte from Uruguay

Fig. 8. Almost complete Mesosaurus tenuidens skull (FC−DPV 2061) from the Early Permian Mangrullo Formation (Northeastern Uruguay) preserved as an impression of the external surface of the roofing bones in original anatomical position. Photograph (A) and interpretive drawing (B). Most sutures can be reconstructed and the component bones are clearly delimited, a type of preservation rarely found in mesosaurids.

Fig. 5 in Unusual environmental conditions preserve a Permian mesosaur-bearing Konservat-Lagerstätte from Uruguay

Fig. 5. Mesosaurid palate (FC−DPV 2462) from the Early Permian Mangrullo Formation (Northeastern Uruguay), including palatine and vomer. Part (A) and counterpart (B). Note the oval area posterior to the choana, probably indicating the presence of a salt gland (see text for additional information). The white arrow marks the posterior boundary of the probable gland. Photographs (A1, B1), interpretive drawings (A2, B2).